SCIENTIFIC ABSTRACT BELYAYEV, V. F. - BELYAYEV, V. I.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000204610019-8
• Release Decision: RIFPUB
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: January 4, 2017
• Sequence Number: 19
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

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Autoxidation of 1-isopropyl-cyclohexene-1 ....

s/5 Po/6 ~/ooo/ooa/oog/o ~6
AO57/Ai26

radical. Hence, the most reactive group in autoxidation is tho methylene group
near the alkyl radical. Tile latter increases the mobility of the hydrogen atom
in the adjoining methylene group. Autoxidation experiments of 1-iso~ropyl_
-cyclohexene-1, at 68�C, during 6 h, carried ou't in the presence of ~he initiators
cobalt stearate, acetate, .%~,aiate, manganese stearate and formiate, or kaolin
shov;ed that the cobalt compounds have the greatest activity, but also docomposa
the hydroperoxide which gm?rates during autoxidation. In the presence of manganam~
,.nd cobalt formiate the rate of autoxidation is smaller th~mn without addizio:-, of
initiator. A new hydroperoxide was synthesized by liquid-phase low-temperature
au%oxidation of 1-isopropylcyclohexene_l and determined as 1-isopropylcyclohezene_
-1-hydroperoxide_6. Autoxldation of 1-ethy!-cyclopentene_l was carried out at
60�C during 5 days without initiator and ~he following ne~ hydroperoxide separated:
!-ethylcyc!opentene-l-hydroperoxide_5. This compound is stable during long-last-
ing storage. ~nere are ~ tables.

Card

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~-LYA~EV, V.F.

Autoxidation of 1.isopropyl-l-cyclohexene and 1-ethyl-1-
cyclopentene to hydroperoxides. ~hidkofaz.okisoneproorgo
soed. no.1:97-104 '61. (~L~J, 15:2)
(Cyclohexene) (Cyclopentene)
(Hydroper~ides)

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KOCHETKOV~ NoKo; BELY~iYEV~�.F.; DUD]2~;~.~ G.S.

Ketovinilation of nitrocyclohe~neo Zhuroobokhimo 32 nOo6:1785-1789
Je '62. (~RA 1~:6)

1. Belorusskiy gosudarstvennyy universitet.
(Cyclohexane) (Vinylation)

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BELYAYEV, V.F.; YATSEVI~lt, N.M.; SOEDLOV, N.A.

Synthesis of chalcones on the base of ~ - chlorovinyl ketcheS. Part 2.
Zhur.oh. kbim. 32 no.6:2022-2025 Je '62~ (MIRA 15:6)

1, Belorusskiy gosudarstvennyy universitet ira. V.I.Lenina.
(Chalcone)

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BEL~A~EV~ ~.F,

Ketovinylation of nitroparafflns.

Zhur. VKItO 9 no. 3~358 '64.
(MIRA 17,9)

1. Belorusskiy gosudarstvennyy universitet imeni Lenina.

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BELYA~V, V.F.
Synthesis of chalcones on the basis of~-chlorovinyl ketoneso
Zhur. ob. kh~. 34 no. 3:861-864 ~!r t6&. (ML~J~ 17:6)
1. Belorusskiy gosudarstvennyy uniYersitet im~ni V.I.I~nina,

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BELYAYEV, V. G.

~ . ~Analysis of a Systam of Caving-In in Layers and ~tho~s of
Perfecting It in the Process of Working Polymetallic and Copper-Pyrite
Deposits.~ Min Higher Education USSR. Moscow Inst of Nonferrous Metals
and Gold imeni M. I. Kalinin, Moscow, 1955. (Dissertation for the Degree
of Candidate in Technical Sciences.)

So; ' z Let s' No 3, 1956

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1.Severokavkmzskiy ogrnometallurgicheakiy institut, Eaffedra
razrabetki poleznyt~h iskopa~emkuh.
(Boring machiner~)

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1. Severolcavkazmki~ goraometallurgtoheekiy inet[tut. Xafedra
rasrmbotkt memtoroshdenty polesn.vkh tmkopayem~kb.
(~adon region--Mining ~negtneering--Oosts)
(Ore dressing--Costs)

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BELYAYE~, V.G.; VEDERNIKOV, I.I.; GONCHAROV, V.N.; PATE!~L"~, A.Kh.;
Rb/.'JANTSEVA, M.B., red.; FORMALI]~IA, Ye.A., tekhn, red.

[Using high-frequency current for defrosting frozen sprat
briquets] Defrostatsiia briketov morozhenoi kiltki tokom
promvshlennoi chastoty. Moskva, Izd-vo zhurnala "Rybnoe
khoztaistvo" VNIRO, 1962. 21 p. (MIRA 17:3)

1. Sotrudniki Kaspiyskogo nauchno-issledovatel'skogo in-
stituta morskogo rybnogo kho~,aystva i okeanografit, Astrakhan'
(for Belyayev, Vederniko�).

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BELYAYE~, V.G.~ BORISENKO, G.A.

Profiling the ball-~eturn channel for ball transmissions.
Stan. i instr. 35 no.6:13-16 Je '6~ (MIRA 17~8)

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.... BELYAYEV~ V.G.

Case of neurodermatftis complicated by a mass attack cf ohicken
mites. Med. pa~az, i paraz, bol. 3~ no.1:116-t17 Ja-F ~65.

]. Prtmorskaya krayevaya prottvochmmnaya stants~ya, Ussurtysk.

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KORNIYENKO, A.M.; SHTEL'MAKHOV, M.S.; GEYLER, Z.Sh.; BERESNEV, V.~.;
KOTLIK, S.B.; GORFINSKIY, EI~.M.; ZEL'DIN, Yu.R.; KURGIN, Yu.M.;
BELYAYEV, V.G.; Z~K, P.S.; ZAYTSEV, A.A.; LI, A.M.$ SKVORTSOV,
LuTTS~-'R.R.; KHVINGIYA, M.V.; NINOSHVILI, B.I.; SE~tENCH~';KO, D.I.;
SUKHANOV, V.B.
Soviet inventions in mechanical engineering. Vest.mashinost~'.
45 no.11:~7-~8 N '65. (MIR~ 18:125

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EELYAYEV, V.I., kand. tekhn.nauk.

Sinking screw piles. Art.der. 20 ne.7:24-25 J1
(Piling (Civil engineering))

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~ELYAYEV, Valentin Ivanovich$ MIR0SHNIC}IENKO, V.D., red. izd-va; SP~LYAR,
s~Ya'.'~-'teklm'."red~[~L~i~lLI~A~ L.N., tekhn, red.

[Practices in planning and analyzing coal production costs] Prak-
tika planirovaniia i ,~-11za sebestoimosti dobychi uglia. Moskva,
Gos.nauehno-te~bn. izd-vo lit-fy po gornomu delu, 1961. 207 p..
(~ 14:6)
(Goal ~d.nes a~nd m{,~{~;--Oosts)

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B~JuTAYEV. V'. !. � k~and. ~ekhn. nauk

F~fect of underloading and successive overloadings, on the fatigue
strength of steels, ~ash. Bel. no.6~94-110 ~59. (~IRa 13~6)
(Steel--Testings)

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PHASE I B00KEXPLOITATION

SOV/610?

� Belyayev, Vasiliy Ivanovich

Issledovaniye protsessa ustalosti metallov (Investigation o�
the Metal Fatigue Process). ~insk, Izd-vo NVSE i PO B~ER,
1962. 109 p. Errata slip inserted. 2700 copies printed.

Ed.: V. T. Nekhay; ?ech. Ed.: A. P. Dubovik.

P~w0~M:' The book may be useful to scientists, machine designers,
and stud~n~.
0OVERAGE: The book deals with metal fatigue and discusses
the effect of various'test conditions on the enduranoe
limit and service life of carbon and alloy steels and
nonferrous metals. The effect of limit load t~pe, the
strain rate, and the size factor (scale effect)is also
analyzed. .Th9 assistance of Professor T. A. Lebedev is
acknowledged. There a~e 55 references:. 52 Soviet, 2
English, and ~ French.

cma

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_

"T.,e use of bbproduct steel powder from ball be&ring proauction in ?owder
metallurgs-."

report submitted for Intl Conf on Powder MetallurG;,, New �ork� i~-!7

Belorussian Pol,,%ecnical Inst~ Minsk.

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AUTHORS:

Kolesnikov,A.G.,and Belyayev,V.I. SOV/155-58-2-42/47
TITLE: On the Crystallization of a ~r oooled Cloud on Interspersed
Artificial Sublimation Center~ (0 kristallizatsii pereokhlazhdennogo
oblaka na iskusstvennykh yadrakh sublimatsii, vvedennykh v nego
putem zaseva)

PERIODICAL: Nauchnyye doklady vysshey shkoly. ~iziko-matematicheskiye nauki,
1958, Nr 2, pp 200-205 (U$$R)

ABSTRACT: The authors consider the ieothermio crystallization of a cloud
consisting of water vapor and water drops cooled to ca. -lO�G,
the micrdstructure of which is independent of the local coordinates,
and in which to a given moment a large set of sublimation kernels
is interspersed. The authors establish a system consisting of six
equations out of which tha number-of appearing crystals, the vapor
concentration, and other charaoteristics of the sublimation process
can be obtained as fuactions of the time.
There is 1 figure, and ~ referenoes, 2 of which are Soviet, and
1 American.

ASSOCIATION~Moskovskiy gosudaratvennyy universitet imeni M.V. Lomonosova
(Moscow State University lmeni M.V.Lomonosov)

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AUtHOr3 ~

TITLE~

PE1LIODICAL~

ABSTP~CTs
~ ~ cr~-llization of a cloud under an influence of CO2 on the

Card 1/2

Kolesnikov, AoG. Belyayev, VoI. SOV/155-58-4-32/34
On the Calculatio~-~ ~'h�-~%e of Crystalline Growth ~f an
Undercooled Cloud Under Influence of Hard Carbonic Acid
(K raschetu skorosti kristalli~atsii pereokhlazhdennogo .
obI~a'pri vozdeystvii na nego tverdoy uglekisl~t-~y)
Nmla~'doklad~ vysshey shkolyo Fiziko-matematicheskiye
nauki, 1958, Nr 4, PP 199 - 206 (USSR)
The authors propose to calculate the process of artificial

basis of %he following simple scheme : The process is under-
stood as a diffusion of ice particles arising under the in~.
fluence of hard carbon digxide, and as the dlaiillation of
water from the drops on the ice crystals� The calculation
according %o this scheme is carried out under the simplest
assumptions (horizontal~ thin~ infinite cloud ; linear
diffusion of CO2 otc). It is proposed to verify experiment-
ally the obtained formulas in order to obtain indications
for those facts which are not taken into account in the/

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On'~he Calculation of the Rate of Crystalline Growth SOV/155-58-4-52/34
of an Unde=ccoled Cloud Under Influence of Hard Carbonic Acid Gas

scheme. A numerical example is given.
There are 2 figures, and. 3 Soviet references�

ASSOCIATIONs Moskovskiy Sosudarstvennyy universitet imeni M.Vo Lomonosova
(~oscow State University imeni Z~oVo Lomonosov) ~
SUBMITTED:' April 5, 1958

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AUTHORSs
TITLE~

PERIODICAL~
ABSTRACT:

Card 1/ $

Kolesnikov, A.G., ~~Ij~..,~ SOV/155-58-5-19/~7
On the Calculation of the Rate of Crystalline Growth of a
Supercooled Cloud Under Influence of Ice-Forming Particles

Nauchnyye doklady vysshey shkoly. Fiziko-matematicheskiye
nauki,1958,Nr 5,PP 102-107 (USSR)
The paper consists of an introduction (section 1) in which
the author refers especially to the papers of V.Ya.Nikandrov~
G.M. Bashkirova, P.N. Krasikov and others, and of 2 further
sections. In section 2 he considers the onedimensional
problem analogously to L'Ref 11_7 : In the starting moment
the ice-forming particles are in a vertical plane and then
diffuse in horizontal direction, whereby simultaneously
crystals are formed on them. For the steam influx to the
crystals the author obtains
q2 = 4*D(u-u2) ld'~2 I n2~2dx2
o -(2)
by similar considerations as in L-Ref 11_7, where j

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19

On the Calculation of the Rate of Crystalline Growth SOV/155-58-5-19/~7
of a Supercooled Cloud Under Influence of Ice-Forming Particles

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(x-x2)2

r max
� 2(x2,~2) = I W~u(x2,~2), r3tg(r~,x2,~2)dr~
o

Here u denotes the steam concentration, r2 medium size of the
crystale in the point x in the moment ~, E the coefficient of
turbulent diffusion, D the coefficient of molecular steam
diffusion, x2 the initial coordinate of the crystal originated
in the moment ~2 ' W the probability of the formation of ice
crystals on the particles, ~ the density distribution function,

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On ~he Calculation of the Rate of Crystalline Growth SOV/155-58-5-19/37
of a SuPercooled Cloud Under Influence of Ice-Forming Particles
r3 magnitude of the parti~le. In section 3 the author tries
to extend the obtained results to the two-dimensional case
occurring in natural situations.
There are 13 references, 8 of which are Soviet, 2 English,
2 Japanese, and ~ American.

A:~SOCIATION: Moskovskiy gosudarstvennyy universitet imeni ~.:.V.Lomonosova
(Moscow State University imeni M.V. Lomonosov)
~;~B~'~TTED: .May 8, 1958 ~/

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:9-58-5-7/15

AuTHoRS: Kolesnikov,
A. G. and Be~, V. I.
TITLE~ The Crystallization of Super-cooled Water Clouds by Freezing
of Drops (O l~istallizatsii pereokhlazhdenno�o vodnogo
oblaka putem zamerzantya kapel')
PERIODICAL: IzvestiyaAkademii Nauk SSSR~ Seriya Geofizicheskaya~
1958~ Nr 5, PP 636-642 (USSR)
.ABSTRACT: Ref.1 considers the process of crystallization of super-
cooled water vapour when crystals arise on sublimation nuclei~
This would occur in seeding experiments, but in natural pro-
cesses it is more likely to occur by freezing of the water
droplets. It is assumed that the cloud is homogeneous (i~eo,
the functions used do not depend on coordinate) so that cal-
culations can be made per unit volume. At the start the cloud
consists of water vapour and drops in dynamic equilibrium. It
is assumed that at a certain time, due to a change in tempera-
ture,, etco~ metaBtability occurs. This moment is taken as the
onse~ of crystallization. Since the saturation vapour pressure
is lower over ice than water, the ice crystals grow at the
expense of the water vapour. This loss of water vapour causes
the unfrozen drops to evaporate and the process continues till
the whole cloud has frozen. The freezing process occurs almost
Card 1/~'nstantly that a seed crystal appesrs. The probability of

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zI~9-58-5-7/15
The Crystallization of-,~uper-cooled Water Clouds by Freezing of
~ropso

appearance seed crystal in unit volume of fluid is a function
of temperature (Ref.2). Taking the process to be isotherma~
" the probability of freezing is proportional to the vol~ue~
Thus~ if n~ drops freeze/unit time from n drops (the s~ne
size) then: n' = ~vn (1)
where ~ = const, v is the volume of a drop. Since the
initial dimensions of cloud droplets are small and crystals
at this stage do not grow to a large sizeG the evaporation of
drops and the growth of crystals can be considered to be con-
trolled by molecular diffusion of water vapour. To describe
this change ~axwell's equation is used for drops (Eq.2) and
crystals (Eq.~)o (Where rI is the radius of-a drop; uI is
the vapour concentration corresponding to equilibrium of vapour
and drops; r2 and u2 are the same quantities for a crystal;
D is the molecular diffusion coefficient for the vapour; ~l
and ~2 are the densities of water and ice; u is the vapour
concentration in the absence of drops and crystals) uI and
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~9-58-5-7/15
~e Crystallization of Super-cooled Water Clouds by Freezing of
Drops�

u2 are considered constant. Since at the initial moment,
the drops are in equilibrium with the vapour, therefore
u(O) m Ul . If the radius of the drops at this moment is R1,
then its radius at any later moment will be given by Eq.(2)
with the boundary conditions Eq.(~). This gives Eq.(5). This
indicates that drops can be divided up according to their
initial radius - drops between R1 and R1 ~-dR1 will

remain similar all their lives and will disappear at the
same time ~' Thus the behaviour of each group can be
calculated separately and the final result got by ~umming~
Let the initial distribution be described by the function
~(Rl) . Then the number of drops at the initial moment in
such a group is: ~(R1)dR1 (6)
Extend the function to fl(u, Rl) so that the number of
drops in the range (R1, R1 + dRl) at any moment v is
equal to: fl(w, R1)dR1 � (7)
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~9-58-5-7/15
The Crystallization of Super-cooled Water Clouds by Freezing of
Drops.
From Eq.(1) we have the number of drops in unit time, from
this group, which turn into crystals (Eq.8). Using Eqo(6),
it is found that fl(~R1) can be expressed by an integral
equation, which is most conveniently expressed in the form
Eqo(9)o At a certain moment ~' the considered group dis-
appear as a result of evaporation. At this moment R1 is
given by Eq.(lO) from Eq.(5). Eq.(lO) permits the initial
radius to be expressed in terms of the moment of disappear-
ance of the drop (R1 = Z(~') ) . To distinguish one group
of similar drops from another group, the initial radius of
the drop is used. Crystals must be defined by two para-
meters: R1 defining the drops from which they arise and
� " the moment of freezing of the drop. The description of
the crystallization process in terms of these two variables
� s' ~nalogous to the.problems,of hydrodynamics in Lagrangian
variables. A function f2(~ , Rl) is introduced so that
the number of crystals formed at time ~" from drops with
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Card 5/~ integrating again for

'9-58-5-7/15
T~e Crystallization of Super-cooled Water Clouds by Freezing of
Drops~ -
initial radii in the range R1 to R1 +dR1 is equal to
f2(~", R1)dR1 . The number of crystals formed per unit time
from this group is given by Eq.(ll). Considering next the
equation for the change in concentration of vapour u(~)
during crystallization, this change/unit time will be equal
to the difference between the total vapour flow from the
evaporating drops and total vapour flow to the growing crys-
tals, Eq.(12). (P1 is the vapour flow from the drops; P2
is the vapour flow to the crystals)� P1 is first found
(Eqol3) and then P2 � This latter can be obtained by in-
tegrating Eq.(3) with the boundary conditions (Eq.14), giving
Eqo(15) which represents the radius of the crystal as a func-
tion of r2(T, T", R1). Eq.(16) gives the flow to a crystal
arising at the moment v" . At ~"
freeze for which Ri~Z(~') E~ . Therefore Eq.(16)
= ~ only those drops can
is integrated for R1 between the limits Z(~") and Rlmax
v" between the limits 0 and ~

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49-58-5-7/15
The Crystallization of Super-cooled Water Clouds by Freezing of
Drops~
Eq~(17) for P2 is obtained. Eq.(12) can be written in the
form Eq.(18), using Eqs.(13) and (17). Thus five equations
(Eqs~ 57 15~ 9, ll ~d 18) have been obtained for five un-
knowns rI , r2 ? nI , n2 and u , which c~ therefore be
found and hence the crystallization process studied� The
initial boundary conditions for the system are that: u = u~ ,
f2 = 0 when � = 0 ; ~" = 0 . Eliminating rl~ r2' fl and
f2 from Eq.(18) by use of the other equations~ an equation
for u is obtained which can be written in the form Eqo(19)
(where ~ is a function of u~) depending on the value of
u in the range ~0, ~, Eq.(19) can be solved by a numerical
method which is discussed below. Taking a small value of
� = vI u is calculated linearly in the region ~, Vl~ and
du/d~ for the point ~l is calculated from Eqo(19). The
process is then repeated until the final value of u is found�
Once u has been found, the other u~o~s can be easily
Card 6/9

APPROVED FOR RELEASE: 06/08/2000 CTA-RDP86-00513R000204610019-8"

"APPROVED FOR RELEASE: 06/08/2000 C]:A-RDP86-00513R000204610019-8

~9-58-5-7/15
The Crystallization of Super-cooled Water Clouds by Freezing of
Drops.
determined. Assuming these solutions are Eqs.(20),(21), (�2)
and (23), then, firstly, it is possible to determine the
overall number of drops nl(~) and crystals n2(~) in the
cloud at any time and, secondly, to determine the density of
distribution by dimensions ~l(~, rl) and ~2(~, r2) at any
time - these functions can be found from experiments compara-
tively easily. The functions nl(~) and n2(~) are obtained
from the definition of the functions fl and f2 '
~(~, rl) and ~2(~, r2) are obtained by considering ~ group
of drops the initial dimensions of which lie in the r~nge
Crl, rI + drl~ where drI is given by Eqo(24). The number
of drops in this group at the moment � is g(~ R1)dR1 ~
which, using Eq.(24) becomes: dr1
~(~, ~l) ~p(~, ~l)
~R1

Card 7/9 Eq.(25) gives the number of drops at time = with dimensions

APPROVED FOR RELEASE: 06/08/2000 ClA-RDP86-00513R000204610019-8"

"APPROVED FOR RELEASE: 06/08/2000 CIA-RDP86-00513R000204610019-8

#9-58-5-7/15
The Crystallization of Super-cooled Water Clouds by Freezing of
Drops.
in the range Itl, rI +~drl~i o From Eqo(22) it is possible
to find R1 = Sl(rl, v.) as follows from Eq~(5). Substitut-
ing in Eq.(25) gives '~1~, Si(r1, ~)~ = ~(rl~ t) . At
~im8 t"